8.4: Review and Additional Resources
- Page ID
- 42691
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Summary
Review and assess your learning. Start with the "Important Terms and Concepts" to ensure you know the terminology related to the topic of the module and concepts discussed. Move on to the "Review Questions" to answer critical thinking questions about concepts and processes discussed in the module. Finally, test your overall understanding by taking the "Self-assessment quiz".
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- weathering
- the breakdown and decomposition of earth material, namely rocks
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- physical weathering
- involves the disintegration of rock materials; breaks large pieces into smaller ones
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- chemical weathering
- decomposition of rocks and sediment.a chemical change occurs and a new product is created from the material that has undergone weathering
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- root wedging
- Plant roots work their way into joints; as they grow, roots create pressure on the sides of the crack enlarging it until the rock breaks apart
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- joints
- rock crevices
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- frost wedging
- occurs when water freezes in rock fractures. As the water freezes it expands putting pressure on the sides of the crack, enlarging it until the rock breaks apart
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- thermal expansion and contraction
- can weaken rock and cause it to disintegrate; expansion upon heating and contraction during cooling weakens rock breaking it apart
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- regolith
- the product of weathering
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- oxidation
- takes place when oxygen reacts with earth materials. Oxygen dissolved in water combines with atoms of metallic elements abundant in silicate minerals.
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- hydrolysis
- an exchange reaction involving minerals and water. Free hydrogen (H+) and hydroxide (OH)- ions in water are able to replace mineral ions and drive them into solution
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- karst
- a Yugoslavian term that comes from a narrow strip of limestone plateau noted for the assemblage of solution landforms
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- sinkhole
- form either from beneath the surface or from the surface down
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- karst window
- forms when the roof above the underground stream collapses in
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- mass movement
- the down slope movement of earth materials under the influence of gravity
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- shear stress
- primarily a function of the force exerted by the weight of the material under the influence of gravity acting in the down slope direction
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- shear strength
- a measure of the resistance of earth materials to being moved
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- creep
- occurs in the top few meters of the surface and is accomplished by expansion and contraction of the soil; slowest of all types of mass movement
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- slide
- a sheet of material that slips over a failure plane ending anywhere from a meter to a kilometer down slope
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- slump
- characterized by a backward rotation of the earth material as it moves along a curved failure plane resulting in a reverse slope
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- earth flow
- fairly slow, occurring over a few hours or so slow that they are almost imperceptible. Accompanied with slumping; no backward rotation; are not confined to channels; are more common in humid areas
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- rock fall
- occurs when blocks of rock shed from a cliff face and collect at the base
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- erosion
- the detachment of earth material from the surface
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- rain splash erosion
- caused by the impact of water striking the surface
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- sheet erosion
- caused by the unconfined flow of water running across the surface
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- rill erosion
- caused by water concentrating into innumerable, closely-spaced small channels
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- gully erosion
- steep-sided trenches formed by the coalescence of many rills
What is the difference between physical and chemical weathering?
- Answer
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Physical weathering processes are those that break rocks into smaller pieces (disintegration). Chemical weathering chemically alters rock-forming minerals into a product (decomposition).
List the effects of chemical weathering on minerals and rocks.
- Answer
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- increase bulk creating stress within rocks
- lower the density minerals
- decreased particle size resulting in increased surface area
- creates more mobile materials
- creates more stable minerals
Compare and contrast hydration and hydrolysis as it relates to rock weathering.
- Answer
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Hydration and hydrolysis involve the absorption of water into the molecular structure of a mineral. Hydration is a reversible process and hydrolysis is not.
What is soil creep and what features of the landscape can be used to tell creep has taken place?
- Answer
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Soil creep is the slow down slope movement of earth material. The process is imperceptible to the human eye. Terracettes, broken retaining walls, curved tree roots, deformed railroad tracks result from creep.
Compare and contrast slumps and slides.
- Answer
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Slumps take place on well-defined failure planes, exhibit rotation of the failed mass, and often form terraces. Slides occur along irregular failure planes with the mass sliding down slope burying the overlying surface with debris.
Explain the process of mass movement.
- Answer
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Mass movement is the down slope movement of earth material under the influence of gravity. Movement occurs when the shearing stress imposed on material is greater than the shearing strength.
What does erosion mean?
- Answer
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Erosion is the detachment of material from the surface.
Describe the process of rain drop erosion.
- Answer
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Rain drop erosion occurs in a series of steps. Initial rain drops soak the surface driving soil particles apart. Subsequent rain drops detach soil particles upon impact. A dimpled surface often results from rain splash erosion.
What is particularly harmful about sheet erosion?
- Answer
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Sheet erosion occurs when the unconfined flow of water across the surface strips thin layers of top soil. It can be imperceptible to the human eye.
Compare and contrast rill and gully erosion.
- Answer
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Rill erosion occurs when moving water is confined to small channels. A gulley is a much larger channel formed from the coalescence of rills
- Backward rotation of a mass of earth material when mobilized is typical of
- slides
- slumps
- rock fall
- creep
- Another term that describes chemical weathering is
- disintegration
- decomposition
- rotting
- fragmentation
- Curved tree trunks, fractured retaining walls, curved roots are typical features of
- slides
- slumps
- rock fall
- creep
- Talus is a deposit associated with
- slides
- slumps
- rock fall
- creep
- Physical weathering
- is typical of warm and wet environments
- results in new mineral products being formed
- increases surface area
- all the above
- Solifluction is a mass movement process in
- the rain forest
- the desert
- the tundra
- the steppe
- _______ erosion occurs when water is confined to small channels.
- rain splash
- sheet
- rill
- gully
- Sheet erosion
- occurs as channeled flow
- in some cases is nearly imperceptible
- occurs when the infiltration capacity of the soil exceeds the rainfall intensity
- all the above
- Karst landscapes develop over _________ bedrock
- sandstone
- limestone
- granite
- basalt
- Conditions favorable for mudflows include
- unconsolidated surface materials
- steep slopes abundant but intermittent precipitation
- sparse cover of vegetation
- all the above
- Answer
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- B
- B
- D
- C
- C
- C
- C
- B
- B
- D
Additional Resources
Use these resources to further explore the world of geography
- OpenAI. (2026). ChatGPT (GPT-4o version) [Large language model]. https://chatgpt.com
- Google. (2026). Gemini (Gemini 1.5 Pro version) [Large language model]. google.com
- Acid Rain and Acid Deposition. (n.d.). In Research Starters. EBSCO.
- Ferrovial. (2025). How acid rain is produced.
- U.S. Geological Survey. (n.d.). Landslide Hazards Program. Retrieved December 12, 2025
- Leong, G. C. (1983). Certificate physical and human geography (3rd ed.). Oxford University Press.
- Maine Geological Survey. (2022, June 6). Bedrock geology - Frequently asked questions. Maine Department of Agriculture, Conservation & Forestry.
- NASA Science. (n.d.). What is lunar regolith? The moon's surface explained. Retrieved December 12, 2025
- National Park Service. (n.d.). Weathering and erosion. U.S. Department of the Interior. Retrieved December 12, 2025
- Ritter, M. E. (2020). The physical environment: An introduction to physical geography. (L. Pitts, Ed.).
- The Physical Environment: Watch PBS NOVA’s Killer Landslides (29:00 minutes) to examine how landslides occur and why they can become major natural hazards. This video explores the physical processes that trigger slope failure, including gravity, water saturation, geology, and land conditions, while showing how scientists study landslide risk and environmental change.
- The Physical Environment: Explore NASA Earth Observatory’s Sizing up the landslide at Bingham Canyon Mine to examine how scientists used satellite imagery to analyze one of the largest landslides in modern U.S. history. This resource shows how remote sensing helps researchers measure landscape change, investigate slope failure, and better understand the environmental processes behind major mass-wasting events.
- The Physical Environment: Explore NASA Earth Observatory’s Mapping landslide hazards in Central America to learn how scientists identify areas that may be vulnerable to landslides. This resource explains how rainfall, topography, geology, and remote sensing data can be used to map hazard risk and better understand where destructive slope failures are most likely to occur.
- Physical Geography Today: Explore USGS’s Real-Time" Monitoring of an Active Landslide above Highway 50, California - USGS to examine how scientists track slope movement as it happens. This resource shows how monitoring tools, geologic observations, and real-time data help researchers understand landslide behavior, assess hazard risk, and support public safety in unstable environments.
- Physical Geography Today: Explore NASA Earth Observatory’s Los Angeles-area landslide expands to examine how landslides can continue to grow over time and threaten nearby communities, roads, and infrastructure. This resource uses satellite-based observation to show how scientists monitor slope movement and landscape change in hazard-prone environments.


